Completed
Intro
Class Central Classrooms beta
YouTube videos curated by Class Central.
Classroom Contents
Disentangling the Controls and Orbital Pacing of SE Atlantic Carbonate Deposition Since the Oligocene
Automatically move to the next video in the Classroom when playback concludes
- 1 Intro
- 2 The last 34 Myr documents the evolution from a unipolar to bipolar world
- 3 Carbonate deposition is an important part of the carbon cycle
- 4 Carbonate deposition in the Atlantic Ocean was poorly understood
- 5 X-Ray Fluorescence Core Scanning unlocks the sediments chemical composition
- 6 We XRF core scanned the entirety of Site 1264 between 2011 and 2018
- 7 The XRF data could help ensure stratigraphic continuity
- 8 CODD: generate composite core photos...
- 9 CODD: ... and composite splice core photos
- 10 We used different tuning approaches from 8-0 Ma because eccentricity was weaker
- 11 The orbital imprint on Caco, deposition shows three distinct phases
- 12 Eccentricity-paced cyclicity (dissolution?) dominates during Miocene warmth
- 13 The MCO may have been preconditioned by early Miocene warmth
- 14 Precession-driven deposition prevails after the mid Miocene climate transition
- 15 High-latitude biomes drove this
- 16 The stronger high-latitude processes coincide with the -8 Ma onset of the LMBB
- 17 The LMBB is globally recognised, but the origins are not yet understood
- 18 The LMBB onset seems synchronous between the Atlantic and the Pacific
- 19 Increased nutrients may come from...
- 20 The global nutrient distribution may reflect regional differences in...
- 21 New insights into the LMBB indicate...
- 22 CODD: Code for Ocean Drilling Data
- 23 Current version CODD 2.1 for IGOR Pro 7 & 8
- 24 A 30 million year CaCO, view of climate, cry and carbon cycle interactions
